Ocean acoustic tomography signals that interact with the ocean surface suffer travel time perturbations which have information on the frequency-direction spectrum of that surface. In this paper, a technique for tomographically estimating spatially varying frequency-direction spectra is introduced. To demonstrate this technique, synthetic signal spectra data were generated using an empirical model for a fetch-limited sea. The synthetic data were then inverted using linear inverse techniques to produce an estimate of the original sea surface spectra. Inverse solutions for both noise-free and noisy experiments are presented and discussed.
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Miller et al. (1989) studied this question.
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